Western Tibet relief evolution since the Oligo-Miocene

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• 作者：Loraine Gourbet^a ; ^{loraine.gourbet@ens-lyon.org} ; Gweltaz Mahé ; o^a ; Philippe Hervé ; Leloup^a ; Jean-Louis Paquette^b ; Philippe Sorrel^a ; Maxime Henriquet^a ; Xiaobing Liu^a ; ^c ; Xiaohan Liu^c
• 关键词：Western Tibetan plateau ; Continental sedimentation ; Geomorphology ; River network ; Karakorum fault
• 刊名：Gondwana Research
• 出版年：2017
• 出版时间：January 2017
• 年：2017
• 卷：41
• 期：Complete
• 页码：425-437
• 全文大小：4002 K
• 卷排序：41

文摘

Relief in Western Tibet is at least 20 Ma old. Western Tibet, presently internally drained, was externally drained during the Oligocene. Modern river network allows to estimate an offset on the Karakorum fault of 210 to 250 km.